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GEOLOGY AND QUANTUM PARTICLE GEO~HEMISTRY AMYOT & BROWNING TOWNSHIPS~ ONTARIO
Claim Blocks 3003160, 3009993 to 3009995 NTS 41 P/06
Donald Hattie ~.J),~ 2 March~ 2005
INTRODUCTION Location and access Previous wOt-k Present WOr-k
GEOLOGY An:hean Protet~ozoic
CONTEl'HS
QUANTUM PARTICLE GEOCHEMISTRY Conifer bark samples
es treatment
Data presentation Comments
REFERENCES
DSET Inc. Invoice for Quantum Particle analyses
Table ~ ..L
Table ..... .£
Table -::0-. ..,:.x.
Table of Rock Units Descriptions of rock Rock sample analyses fot- Au and Ag
es
Table 4- Quantum Ie analyses for conifer barks Table ;:.
His
Map 1 j1ap 2
'< -..J
Map 4-Map 1l:::
...;
!'lap 6 7
Map 8 Map 9 1'1a.p 10 t'iap 11 Map 12 Map 13 Map 14
Quantum particle analyses fot- soils
fOr- quantum
1 location Claim location
e data
Geology: Parts of and Browning Twps~ Geo ~ Grid A-2, Browning Twp~ Bark sample locations and type Quantum les in Barks Cu~ Pb, In, Ag Quantum particles in Barks Au, Sb, Hi, StQuantum particles in Barks Ni~ Co, As,S Quantum particles in Barks Ba, B, Tl, Ga Soil Quantum Quantum Quantum Quantum
locations pat-ticles in p<:!u'-tic 1 es in pat-ticles in particles in
and Soils Soils Soils Soils
desct-iptions Cu, Pb, In, Ag AU lI Sb, Bi~ Hg Ni., Co, r._
H!::r, S Sa, B" Tl, Ga
Page
1 1 1
2 3
4 4 5
5
6
1:500~OOO
1:.20,,000 1. :: 10 ~ 000 (tipoc:.kel) 1: 5,000 1~ 5,000 1: 5!tO(}()
1: 5,000 1 :::5,000
1 ~ .... 1.: 1: .1;; 1:
1~ 5,000 5,000 5,000 5~OOO
5,000 5,000
GEOLOGY AND QUANTUM PARTICLE GE~DC!-lEIM I STR'l AMYOT & BRmsJNING TOWNSHIPS~ ONTAHIO
Claim Blocks 3003160, 3009993 to 3009995 NTS 41 Pf06
Donald Hattie 2 March~ 2005
INTRODUCTION Location and access
These four claim blocks are centered at 25 km south-southeast from Shin Tree~ The Amyot section can be entered by car along forestry roads off the Meteor Creek Road. For that section, we rented accoIDoaation at the cabin of Wolfgang Foehr of Hanmer, Ontario~ The distance to that camp is 52 km from Shining Tree (43 km from highway 560). The Browning section can be f-eached by cat- on a 2004 forestt-y r-iJao off the Sandy Lake Road ~ 56 km from Shining Tree {(47 km from 560). For the Browning part~ we on the north side of an unnamed lake which we have been calling Figure Eight Lake.
Much of the Browning section is covered sand dunes, with on a few s'=attet-ed outcrops~
sand plains a.nd The part
also has sandy overburden, but containing glacially transported boulders~ and there is a sca.t
of the claim blocks have been cleat- cut in the past decade" and more cut blocks have been contractors have been commendably
Previous work
The timber claim
The sectimi! is at the 'south tip of a maj or ect Ltd which involved airborne and ground
csz Diamond drill on geophysical features to the north defined north trending belts of felsic and mafic volcanics hosting volcanic exhalative massive sulphides with sub-economic base metal content. On grid A-2 in the claim block 3003160~ only pulse EM was performed (Tindale, 1999, Assessment File CO-2460;; 20 and 21)~
The area was mapped 2003 G.W. Johns with the result lished as Ontario Geological Survey Map p~ 3531z
The present four claim blocks were acquired by staking because Dr. C.G. Cheri ton considered the ar-ea fa\lorable for veins 7 in a fractured zone. just under the Nipissing diabase sill which lies to the southeast. with this in mind failed to find any vein material in the poorly target areas.
Attention was drawn to the extensive work Falconbridge
1
Ltd. to the nm-tn 7 and to the fact that the most southerI)-" geophysical features, which are blanketed by sand, remain untested An ¥-,las made to evaluate the pulse EM features
"deep sour-ced" quantum par-ticle
Johns" map shows volcanic rocks and quat-tz porph),,·-y e}~ southwest in Amyot and Hodgetts Twps!, so prospecting was done there. Attractive felsic volcanic flows with "grid jointing", similar to Noranda area~ was observed, and also coarse felsic fragmental volcanic rocks, but no base metal sulphides were found. cDr~tain
ARCHEAN Volcanic suite
Three pyritic volcanic samples did not
Not efiough time t.'\ias spent to SOt-t out the of this suite~ then: any 1 is aSSLtfned 5
Only at the southwe·st Cot-fiet- of Block 3009994 was a general riorthe,ast stt-ike
Felsic volcanics
2
Several large c.utcrops near the road in ~Jest-cefitr-i3.1 3009994-are siliceous grey felsic volcanic flows with nodular devitrification~ and laced with a stockwork of quartz films which stand out on the weathered surface~ These are very similar to the t-id jointing" in the NOr-anda camp. 3 mm are present.
Quartz phenocrysts 1 to
Some massive volcanic outcrops have been labelled intermediate volcanic where where appear less siliceous~ and lack These rocks become granUlar,
granitic contacts, with scattered biotite~ and f may be coated by chlorite, or fibeFous bole.
Near the southwest corfiet- of Block 3009994, several are felsic or intermediate volcaniclastics~ Some are poorly bedded grey fine grained tuffs or water lain volcanic debris. One and a few glacially boulders are coarse felsic fragmentals; with grey felsic clasts to several decimeter-s.
Mafic volcanics
Though mafic vc.lcanic xenoliths ,;u-a common intrusives~ outcrops of these rocKs were small. green~ chloritic, and severely llised. features were recognized.
in the granitic The [-ocks cU'-e
No volcanic
•
Near the northwest corner of Block coarse black weakly magnetic mafic pyrrhotite is cut by granodiorite. The
the gabbt-o.
Gf-ani tic sui te
3009994, one outcrop of with a few of
is chilled
The parent magma may have been a biotite leucogranite which appears in scattered Near the volcanic areas, much of the intrusive suite grades through hornblende-minor biotite granite to hornblends granodiorite {all handspecimen identification)~ with numerous 1 to 10 em rounded xenoliths of gn=~en mafic '-=,olcanic= It appears that the magma was modified b)f
digestion of volcanic rDcks~ Some joints are coated by epidote; and some are reddish stained.
Very few leucocratic few centimeters thick~
PROTERDZIC
forma.tion
its were seen~ always only a
3
The lowest unit~ which appears to rest on Archean granitic rock and mafic volcanic, is a few meter thick very coarse boulder conglomerate with greenish sand matrix. The clasts up to 05 ill;
mostly rounded but some are angular, are mainly granitic rocks and mafic volcanics~ y locally derived. The rock is stream ited but bears a close resemblance to the Gowganda tillite, from which it may have been sourced. Upwards, the conglomerate is interbedded with greenish to dull maroon conglomerate, coarse sandstone~ and some grey-green to maroon fine sandstone and siltstone.
her in the Gowganda there are flaggy green-grey fine to coarse sandstone, with occasional 2 cm granitic pebbles. One such pebble had sever-al pet-cent pyri teo Scatten:! specks of pyrite are present in the sandstone in some outcrops.
Lorrain formation
The few outcrops in the of the project claims are very clean white quartzite and pebble conglomerate. Quartz pebbles are up to 5 cm diametet-. Bedding is pn".'sent variation in grain size, but its orientation is not easily de'tenTdned in broken au wi th 1 i chen cover =
Mafic dykes
There appear to be at least two ages of diabase The presumed c ones al~e nOt-ttl-striking massive, dark
diabase with brown weathering and are of pyrrhotite are present.
1- '" 7
4
magnetic~
Some finer grained ~ less inagnetic black diabase dykes may be c=
Most rock somewhere have reddish (hematite) stains which from joints: This featuneo is most not.icable in the granitic suite It seems likely that these are groundwater deposits below ancient weathering surfaces, rather than rothermal alterations.
QUANTUM PAHT I CLE GEOCHEf~-! I STRY Conifer Bark Samples
es were scraped from the bark of conifer trees using a horse curry comb into a plastic mesh feed bag and then transferred into H ht " feed freezer bags.
Between 30 and 50 trees were along 30 meters of grid line~ In most cases, the trees were ioeJithin 5 meters ef the lins, but in cases ~'Jhere matl.u-e tr-ees I>JelC-e scarce~ sampling e;{tended to as much as 40 meter-s from the line~ Jack was the most common tree pe, with ficant amounts ef l-ed spt-uce on some lines= Balsum fit- was an impot-tant tree species in on a few samples, on the mid of Line 1820N and t.he west end of LiriE'S 23{)(Jt~ and 3(H)(lr..f ~
Bark samples were delivered to Howard Lahti in Fredericton~
Soil Sa.mples
The whole area sampled is underlain by post-glacial wind blown very fine sand and silt, on which is developed a cal soil profile: black decayed humus~ in some cases with ash and charcoal at its base; g leached "An zone; red brown~ orange or yellow "BY zone grading downward to paler DC" zone. At some sites a Line 2700N and 3000N, thel'""e is a less than 1 em thick dark brown layer at the of the HB n zone. The mid part of Line i820N is ect to annual flooding from Meteor Creek which near that line, so that the humus layer is mixed with fine and and silt from the Creek, and it is e that the material sampled (Samples FELS-4 to -8) t-Jas also deposited recently the Ct-eek d
A 40 em disc I.-'¥as from the root-l humus la}let-an army-style trenching tool, the nAn horizon was
away and the top 10 em of the as" horizon~ about 500 grams, was collected into conventional paper sample , as n=~commended by !-ii;:J\o'Janj Lahti. The samples were delivered to Hof.~ard Lahti's laboratory in Fredet-icton, N=B.
Labora Trea.tment
Howard Lahti uses a proprietary process to extract "quantum dots" or "quantum les" (see Stace!, .1988, Duncan & .1989, Roukes, 2001 and an paper Hochella and Madden~ 2005; • In La.hti and others, 2003~ page 5, it is mentiDned that the particles are collected by a cal process.
FDt- coni fer the
es, the material is asned as well as extraction process.
The of HO~;jard Lahti's processes were forwan::led to ACME Analytical Laboratories Ltd. in Vancouver for analyses ICP-ES and ICP-MS t Induced ed Plasma emission spectlrometry and mass spectrometry) following a hot aqua regia digestion.
very low detection limits for 37 elements. Analytical are in Tables 4 and 5.
Data Presentation
rams were for all elements which to show significant variation, for each of the soil and bark
5
analytical Many of the distributions are bimodal. Most of these are on a logarithmic base which the visual impact of her values, but there are only few results that are obviously outside the range of the total population(s}.
The ne>ft considered of most significance, another set for the bark samples
Comments
map ots of the elements one set for the soil samples (Maps 5 to i4).
show that there are very few distinctly anomalous results. the elements and indicators for theffi~ only a gold in barks and soils, one silver~ one arsenic, one antimony, one suI , one strontium and a few barium in barks, and one antimony, one suI ~ one bismuth and four boron in soils fall distinctly outside the population clusters. A few iron~ manganese~ chromium and vanadium values are also distinctly anomalous. However, the Line plots show that an encourag proportion of the relatively high values are in pf-o~{imi ty to the Timed (Pulse) EM fea.tures intet-pr-eted by Falconbr Also, it is en that there is some confirmation of anomalies between the two e media.
The pattern on Line i920N differs in that the two ends of the line are distinctly higher in most elements in both soils and barks~ compared to the central part of the line, near Meteor Creek~ The soils are quite recent, from floods from the Cr-eek • The bad<. s may have 1 o~... me ta 1 s ei ther because of the. highE4r ion of balsum fi .. -, Ot- due to the over-but-den below
being water saturated and inhi particles.
the movement of
The drop off in values for most elements going west along Line 3000N ma.y be due to increasing thicknes of the sand-si 1 t dune or to distance from the Pulse EM feature. There is also an increase in balsum fir in the bark samples toward the west on
SUMMARY
over projected fracture zones in the Proterozoic rocks failed to find any sulphide vein material in the poorly
Attractive felsic volcanic flows with "grid jointing"~ similar to Nor-anda area, was observed in the southwest
of claim block 3009994 in Amyot Twp. Also, coarse felsic fragmental volcanic rocks are present near 3, but no base metal suI irJere found = Thn?e tic volcanic samples from near Post 4 of that laim block did not contain gold Dr silver.
The cal results are not dramatic~ but give some encouragement that there are concentratins of base metals~ silver and gold associated with the Pulse EM features interpreted by Falconbridge from the data collected by Rayan Exploration Ltd (Ray Miekle) of Timmins in March, 1996 ( 20 and 21 in Assessement Peport CO-2460~ Tindale, 1999J<
REFERENCES
Cameron, Eion M=~ Stewart M= Hamilton~ Matthew I~
Gt';iendy E.I'L Hall and Beth McClenaghan, 2004 deeply om-ied
Geochemistry: Exploration, 7-32
ts using geochemistry: Environment, Anal , vol.
Duncan~ Michael A., and Dennis H Rouvray~ 19B9, Microclusters: Scientific American Dec.~ 19B9~ p 110-115
Johns, 8.W:~ 2003 Precambrian Geology, Shining Tree South area: Ontarian Geological Survey~ Pn?liminary j"lap P,,3531, scale 1:::,;,)!,OOO
Lahti, Howard, 2003 Testing of deep pene geochemical technology: NQB~ Department of Natural Resources~ Minerals, Policy and Flann Division~ Open File 2003-3, 106 pages
Lahti~ HOIi'-~ardJ' S.H. McCutcheon and M_A. Parkhill, 2003 • Reconnaissance and detailed GPX B-horizon soil and QPVX
geochemistry in the Bathurst Mining Camp,
p
Gloucester and Northumberland Counties!, New Brunswick: N.B~ Depar-tment of Natural Resources, Minerals!, Policy and Plann Division, File 2003-8, 101 pages plL~s maps
Roukes, Michael, 2001, Plen 48-57
of Room Indeed: Scientific American, Sept , 2001~ P
Stace~ Tony~ 1988, How small is a solid?: Nature~ Yol.331, p 116
Tindale~ J.L=, 1999~
ASSESSMENT REPORT~ Sheard~ Amyot, Browning and Ogilvie ,Shin Tree Arae, Larder Lake Division,
NTS 41 P/Ob; (final of work Falconbridge Ltd.,
7
plus review of geophysical data Eberhard Berrer) Ontario Assessment CO-2460
ication to watch for:
Hc,chella, Michael F, Jr, and AndreirJ S. I"iadden~ 2005", The ce of cies and their unusual properties in iments and soils from heavy metal-contaminated sitesi ELEMENTS, An International ine of Mineralogy~ Geochemis , and Petrology, volw 1~ No 4, planned issue for t$;y 2\)i)5
111
FAX Deep Search Exploration Technologies Inc
115 8 Woodstock Rd Fredericton NB E3B 7S 1
Tel: 506458-0982 E-mail: hlmv(t4nb.svmpatico.ca
To: Don Hattie From: Howard Lahti Date: Nov 2, 2004 Subject: Invoice for QPX and QPVX Samples HST Number: 895956415 Re0001
Hi Don, The following is the charges for the work done by DSET in Oct 2004. Ontario Project 45 soils FELS-Ol to 45 and 33 Bark FELB-Ol-33.
a) QPVX 33 samples $30/sample
b) QPX 45 samples: $25/sample =
TOTAL $ 2432.25
Total Amount Of This Invoice $ 2432.25
Respectfully Submitted,
~~ Howard Lahti
15%HST subtotal
15%HST subtotal
$ 990.00 148.50
$ 1138.50
$ 1125.00 168.75
$ 1293.75
PROTEROZOIC
Diabase kes
Hu.r-onian Superyt-oup Len-rain formaion
TABLE 1 - Rock Un~ts
Mafic, magnetic diabase
White quartzite and pebble conglomerate
Gowganda fOrmation Grey green flaggy fine sandstone, with t-are granite pebble'!:.
Oldet- diabase?
ARCHEAN
Sf-ani tic sL~i te
Volcanic suite
Felsic volcanics
Maroon siltstone and fine to coarse sandstone and ly sandstone; with dull green reduction patches Very coarse conglomerate with pebbles~ cobbles and boulders mainly of granitic and mafic volcanic rocks (derived from Gm-Jganda ti II?)
Some dykes are only !!-leakly magnetic
Varries from biotite leucoQranite. to hornblende granodiorite~ mafic voicanic ~{enoli ths ai-e common ~ Few centimetetthick aplite kes
Black, medium to coarse mafic gabbro; very weakly ,cut granite
Relative ages not established; cut and metamorphosed by granitic suite Massive siliceous flows, often with up to 3 mm ; parts with devitrification nodules and ; parts gridded by films Felsic to intermediate volcaniclastic rocks, poorly bedded; from fine grained to decimeter sized clasts
\,fol canics Dull grey;; less '!:.i liceous; may haVE' chlorite or amphibole seams on fractures where near granitic rocks
Mafic volcanics Dark green metabasalt; common as centimeter sized xenoliths in granitic suite
•
TABLE 2 - Assayed Rocks
~~'=<~~tative chips were collected across pyri volcanic rock outcrops
Field No. Weight Width
A-2 1.5 kg
A-3 0.8 kg
A-13
8 m intermediate volcanic with disseminated biotite; less than pyrite evenly distributed~ partly disseminated and partly as grains along fractures NAD 27 Zone 483350E 5241780N
5 m Grey siliceous rhyolite?; minor carbonate alteration; minor amphibole on fractures:; less than 1% LIP to 2 mm pyrite irregularly distributed~ mainly in ft-actures
2 m Siliceous intermediate volcanic, lLne to medium grained, sheared with minor
blobs; chlorite {after biotite?); bele-very magnetic
pyrrhoti te on fractUl'-eS!i less than 2 % pyrite and te irregularly distributed NAD 27 Zone 17 483800E 5241800N
. ; I I
Table 3
Swastika Laboratories Ltd .Established J 928 .
Assay Certificate
Company: HARTE GOLD Project: Attn: T. O'Connor
Assaying - Consulting - RepreSentation
We hereby certify the following Assay of 14 Channel samples submitted FEB·OI-05 by .
Sample Au Au Check Ag Number g/tonne s/tonne PPM
.-- --- - -------- - ... ----------73001 2.36 2.41 0.1 73002 0.86 b.l 73003 2.44 2.33 0.1 73004 3.34 3.31 0.1
STD OxK18 . 3.40
--------~---~------------
Certified by .
5W-0142-RAl
Date: FEB-03-05
TobIe if. : 6(tianlr;m ;varleles In btu:"h
ACME ANALYTICAL LABORATORIES lTD. 852 E HASTINGS ST. VANCOUVER BC V6A 1R6 PHO Deep Search Expl. Technologies Inc. Acme file # A406082 Received: OCT 4 2004 * 36 samples in this disk file. Analysis: GROUP 1 F - 0.25 GM ELEMENT Mo Cu Pb Zn Ag Ni Co Mn SAMPLES ppm ppm ppm ppm ppb ppm ppm ppm FELB-01 6.87 627.64 585.54 1086 938 254.9 9.1 1424 FELB-02 5.44 687.14 568.37 1469.9 1010 261.4 8.8 2675 FELB-03 6.29 701.95 734.45 1328.2 1099 265.5 9.4 4163 FELB-04 5.38 707.89 693.65 1672.8 896 213.1 8 4907 FELB-05 7.18 842.09 593.01 1566.2 1102 252.4 9.5 7032 FELB-06 6.1 697.78 619.48 1561.6 1039 210.9 7.5 6290 FELB-07 7.49 694.59 584.05 1544.3 1000 227.3 8.1 4807 FELB-08 6.45 769.11 829.84 1833.2 923 228.9 8 5101 FELB-09 4.75 596.59 639.2 1983.5 800 194.5 7 5589 FELB-10 5.19 661.75 550.52 1983.6 821 173.1 6.9 4675 FELB-11 1.36 267.78 179.97 2667.3 560 62.3 4 5508 FELB-11 T 1.49 300.63 204.01 2590 655 63.8 4.5 5510 FELB-12 2.19 336.83 277.72 2104.2 491 87.1 4.6 4963 FELB-13 1.21 253.85 108.75 1841.5 558 71.3 8 8946 FELB-14 2.34 210.59 115.95 812.3 419 62.6 11 7402 FELB-15 1.11 209.15 118.8 1273 514 56.6 4.7 3048 FELB-16 4.16 485.68 463.2 1362.5 613 162.9 6.6 3688 FELB-17 1.12 173.06 91.13 1165.1 480 39.5 4.2 9514 RE FELB-1;' 1.15 177.9 93.88 1220.3 480 40.3 4.9 9521 FELB-18 1.33 205.52 118.93 1344.4 492 50.9 4.1 9933 FELB-19 2.77 463.38 359.73 1575.3 668 120.5 4.9 6146 FELB-20 4.4 669.83 597.56 1907.1 980 199.9 6.6 6172 FELB-21 4.51 572.15 694.11 1907.8 836 191.6 6.7 5302 FELB-22 3.42 513.17 584.89 1642.4 ~1342 170.4 5.9 5824 FELB-23 2.89 726.17 442.53 1675.6 564 122.4 4.8 6677 FELB-24 3.73 442.48 530.31 1469.9 787 127.6 5.4 4978 FELB-25 4.89 542.8 698.41 1632.9 907 141.2 5.9 5035 FELB-26 4.27 504.54 585.89 1572.4 875 138 5.4 5738 FELB-27 5.55 649.39 693.47 1642.6 1021 205.5 7.5 5238 FELB-28 5.09 445.41 523.77 1476.7 865 157.6 6.3 3620 FELB-29 5.52 575.49 624.92 1633.5 1044 205.4 7.4 7416 FELB-30 4.43 524.53 540.01 1674.3 961 195.5 6.8 9489 FELB-31 5.06 681.71 613.36 1772.2 1036 274.2 8.8 4790 FELB-32 2.59 404.3 319.39 1642.8 964 140.9 5.3 11338 STAN DAR 12.41 142 24 140 272 26.2 11.1 818 FELB-33 1.8 279.21 249.19 1853.8 510 87.5 4.1 12129 STAN DAR 12.34 142.59 24.72 140.6 278 24.2 11.2 802
NE(604}253-3158 FAX(604}253-1716
ELEMENT Fe As U Au Th Sr Cd Sb SAMPLES % ppm ppm ppb ppm ppm ppm ppm FELB-01 1.64 9.7 1 515.7 2.4 200.3 16.37 5.44 FELB-02 1.71 13.4 0.7 412.8 2 217.1 16.24 5.26 FELB-03 1.79 14.8 0.9 364.7 2.3 327.6 19.93 6.37 FELB-04 1.4 16.4 0.7 382.2 1.5 450 22.69 6.87 FELB-05 1.55 -.23.2 1 360.1 1.8 448.9 24.33 9.28 FELB-06 1.42 15.6 0.8 '-11- 890.8 1.6 511.7 22.1 6.96 FELB-07 1.53 17.1 1 250.4 1.9 540.2 20.55 8.85 FELB-08 1.36 14.7 0.9 354 1.6 588.1 26.85 7.63 FELB-09 1.2 12 0.7 410.9 1.3 568.6 26.02 6.15 FELB-10 1.34 15.4 0.8 411.6 1.4 252.1 21.46 6.73 FELB-11 0.39 3.8 0.2 166.8 . 0.4 683 10.24 ~ 1.53 FELB-11 T 0.37 5 0.2 354.7 0.3 699.2 19.24. 1.61 FELB-12 0.6 5.3 0.4 164.2 0.7 494.2 16.75 2.54 FELB-13 0.55 18.4 0.3 61.1 0.5 432.2 21.27 0.78 FELB-14 ~}"'" 9.42 16.5 0.3 87.1 1.1 166.5 19.26 1.65 FELB-15 0.55 2.3 0.2 66.7 0.8 295.8 14.1 0.92 FELB-16 1.12 11 0.7 124 1.3 186.5 19.96 5.02 FELB-17 0.56 4.5 0.3 35.5 0.6 455.9 17.9 0.71 RE FELB-17 0.52 4.1 0.3 37.5 0.6 496.6 15.96 0.74 FELB-18 0,4 4.8 0.2 62.5 0.3 677.6 16.05 0.97 FELB-19 0.67 6.7 0,4 338.1 0.6 686.1 17.87 3,44 FELB-20 1.15 11.3 0.7 155.8 1.1 497.6 ~29.22 5.38 FELB-21 1.13 11 0.7 148.9 1.2 483 -"" 28.79 5.78 FELB-22 0.86 8.7 0.5 286.5 0.9 532.7 22.9 4.31 FELB-23 0.66 7.1 0,4 548.1 0.7 515 24.88 3.36 FELB-24 0.9 9.9 0.5 229.7 1.1 373.8 18.24 4.81 FELB-25 1.11 11.1 0.6 ~"" 678 1.5 262.1 21.64 6.01 FELB-26 1.1 10.1 0.6 401 1.2 285.3 21.28 5.24 FELB-27 1.26 12 0.7 241.3 1.6 322.1 19.76 5.93 FELB-28 1.22 8.1 0.7 310.2 1.7 380,4 14.91 4.99 FELB-29 1.22 10 0.8 276.3 1.5 415.5 21.97 5.76 FELB-30 1.05 9.7 0.6 151.9 1.2 455,4 23.72 4.63 FELB-31 1.25 9.5 0.6 176.7 1.6 373 25.97 4.51 FELB-32 0.68 7.8 0,4 162.1 0.7 566.1 24.83 2.7 STAN DAR 3.04 18.2 6.2 45 2.6 44.8 5.5 3,49 FELB-33 0.36 5.2 0.2 256.3 0.3 ~> 935 21.9 1.93 STAN DAR 2.99 16.9 6 41.6 2.7 44.3 5.56 3.41
ELEMENT Bi V Ca P La Cr Mg Ba SAMPLES ppm ppm % % ppm ppm % ppm FELB-01 --r_ 7.41 44 23.13 0.86 12.6 28.4 0.66 340.7 FELB-02 6.5 42 19.1 1.202 11.5 26.2 0.88 357 FELB-03 6.57 48 19.84 1.327 13.5 28.1 0.96 184.5 FELB-04 5.15 44 21.78 1.269 10.6 26.3 1.01 138.6 FELB-05 6.7 -r_ 56 22.32 1.704 13.7 25.6 1.09 _.!f'.,> 803 FELB-06 5.25 43 20.83 1.408 11.2 25.8 1 122.2 FELB-07 6.34 51 19 1.478 13.7 27.4 1 134.8 FELB-08 5.49 46 19.94 1.495 12 26.5 1.07 125.1 FELB-09 4.19 38 20.93 1.236 9.5 19 0.98 135.3 FELB-10 4.76 43 19.67 1.368 9.2 21.3 1.09 325 FELB-11 1.03 11 28.65 0.691 2.6 7.1 0.76 235.3 f)
FELB-11 T 1.46 11 28.82 0.744>: 2.7 6.1 0.77 ...... 1888.8 FELB-12 2.19 19 25.91 0.706 4.8 11.6 0.82 199.5 FELB-13 1.14 11 20.81 0.747 4 9.5 0.83 54.3 FELB-14 1.08 13 --"'P< 8.1 0.814 5.5 20.9 0.66 489.4 FELB-15 1.1 12 15.37 0.699 3.7 12.4 0.57 --.610.6 FELB-16 3.68 33 15.24 1.03 8.3 20.7 0.83 150.3 FELB-17 0.94 10 22.17 0.625 4.2 10.5 0.53 184.6 RE FELB-1 0.89 10 23.63 0.672 \< 4.2 10.4 0.52 227.9 FELB-18 1.03 8 26.72 0.651 2.4 5.2 0.49 129.3 FELB-19 2.52 20 24.79 0.994 4.9 17.3 0.72 165 FELB-20 4.5 34 21.22 1.269 8.7 32.1 0.89 142.2 FELB-21 4.56 37 20.72 1.251 8.9 22.3 0.93 140.5 FELB-22 3.37 27 22.92 1.196 7.1 18.9 0.89 150.9 FELB-23 2.75 21 23.59 1.023 5.4 -75.7 0.93 135.9 FELB-24 4.1 27 22.78 1.098 6.8 19.9 0.81 144.2 FELB-25 4.84 34 20.98 1.272 8.3 24.8 0.99 139.8 FELB-26 4.47 33 22.47 1.179 7.9 26.9 1.02 167 FELB-27 5.53 37 22.21 1.17 8.8 28.6 0.92 143.3 FELB-28 3.95 33 21.4 1.01 9.2 30.8 0.85 138.3 FELB-29 4.,86 38 22.94 1.035 9.4 30.9 0.8 129 FELB-30 3.9 32 24.65 0.961 7.7 23.8 0.77 130.5 FELB-31 5.56 34 23.4 1.097 8.9 24.6 0.89 160.4 FELB-32 2.54 19 25.99 1.066 4.7 16.5 0.71 165.7 STAN DAR ,6.16 59 0.78 0.103 13.2 181 0.7 137.3
~
FELB-33 ! 1.58 12 29.26 0.704 2.9 9.7 0.69 232.2 STAN DAR ·--.3>5.75 60 0.77 0.091 12.8 176.2 0.65 135.5
ELEMENT Ti B AI Na K W Sc TI SAMPLES % ppm % % % ppm ppm ppm FELB-01 0.025 123 1.76 0.056 1.51 0.9 2.3 0.69 FELB-02 0.026 158 2.55 0.061 2.59 0.9 2.3 1.45 FELB-03 0.027 183 2.77 0.06 3.14 0.8 2.4 0.91 FELB-04 0.021 211 3.3 0.062 3.21 0.7 1.9 0.08 FELB-05 0.027 -~ 267 3.25 0.072 3.64 0.8 2.3 0.98 FELB-06 0.024 193 3.34 0.062 3.39 0.7 2.2 0.11 FELB-07 0.028 178 3.64 0.065 3.44 0.8 2.5 2.05 FELB-08 0.025 185 3.62 0.055 3.38 0.7 2.1 0.19 FELB-09 0.022 165 3.12 0.056 2.83 0.5 2 1.39 FELB-10 0.022 166 2.92 0.053 2.97 0.6 2 0.73 FELB-11 0.009 179 0.64 0.028 2.14 0.2 0.6 0.05 FELB-11 T 0.009 200 0.66 0.03 2.21 0.1 0.8 0.08 FELB-12 0.014 154 0.93 0.041 2.07 0.2 1.2 0.11 FELB-13 0.015 145 0.44 0.04 3.06 <.1 0.9 0.76 FELB-14 0.023 81 0.56 0.033 2.7 0.2 1.4 1.13 FELB-15 0.017 113 0.46 0.024 1.87 0.2 0.8 0.82 FELB-16 0.022 139 2.25 0.037 1.94 0.6 1.6 1.63 FELB-17 0.015 103 0.41 0.023 2.39 0.1 1.1 1.05 RE FELB-1 0.015 113 0.38 0.023 2.3 0.1 1 1.03 FELB-18 0.008 122 0.37 0.018 2.32 0.1 0.7 0.52 FELB-19 0.013 147 1.68 0.026 2.57 0.3 0.9 1.02 FELB-20 0.02 161 2.93 0.036 2.83 0.5 1.7 1.83 FELB-21 0.02 144 2.95 0.036 2.84 0.5 1.6 2.2 FELB-22 0.016 119 2.25 0.03 3.03 0.4 1.3 1.67 FELB-23 0.012 134 2.11 0.03 2.63 0.4 1 0.73 FELB-24 0.016 143 1.73 0.043 2.81 0.4 1.4 1.17 FELB-25 0.018 149 2.28 0.05 2.77 0.6 1.5 1.63 FELB-26 0.018 149 2.21 0.048 2.64 0.5 1.6 1.49 FELB-27 0.019 160 2.22 0.046 2.42 0.6 1.6 1.75 FELB-28 0.02 179 1.93 0.046 2.4 0.5 1.8 1.35 FELB-29 0.02:1 185 1.79 0.045 2.72 0.6 1.7 0.99 FELB-30 0.017 189 1.79 0.038 2.44 0.5 1.4 1.06 FELB-31 0.019 169 2.22 0.047 2.66 0.7 1.5 1.22 FELB-32 0.013 180 1.17 0.031 2.93 0.3 1 1.71 STAN DAR 0.105 17 2 0.037 0.15 5.4 3.4 1.08 FELB-33 0.007 189 0.69 0.022 2.44 0.2 0.6 0.52 STAN DAR 0.104 17 2.02 0.036 0.14 5.3 3.4 1.05
ELEMENT S Hg Se Te Ga SAMPLES % ppb ppm ppm ppm FELB-01 2 <5 15.5 0.43 4.1 FELB-02 2.14 <5 15.4 0.49 4 FELB-03 2.4 <5 18.2 0.45 4.8 FELB-04 2.7 <5 17.6 0.43 3.8 FELB-05 2.73 <5 19.7 0.53 5 FELB-06 2.69 <5 17.8 0.34 4.3 FELB-07 2.61 <5 20.2 0.34 5.4 FELB-08 2.34 <5 16.9 0.31 4,5
FELB-09 1.98 <5 14.3 0.29 3.6 FELB-10 2.52 <5 15.9 0.28 4 FELB-11 S 0.91 <5 , 3.8 0.09 1.1 FELB-11 T -, 1.71 <5 5.4 0.08 1.1 FELB-12 1.38 <5 6.5 0.12 1.7 FELB-13 --?- 4.73 <5 3.3 0.24 1.4 FELB-14 0.71 <5 2.1 0.05 2,5 FELB-15 0,75 <5 2,2 0,07 1.2 FELB-16 2.16 <5 12.2 0,23 3 FELB-17 1.25 <5 2,5 0,07 1.4 RE FELB-1 1,17 <5 2.6 0.09 1,5 :":
FELB-18 1.69 <5 3.4 0.12 1.3 FELB-19 1.71 <5 9.3 0.15 2.1 FELB-20 2.17 <5 14 0.26 3.5 FELB-21 2.31 <5 15 0.22 3,5 FELB-22 2.11 <5 12.4 0.25 2.5 FELB-23 1.89 <5 10.1 0.19 1.9 FELB-24 1.98 <5 12.4 0.2 2.7 FELB-25 2.1 <5 13.1 0.23 3.1 FELB-26 2.09 <5 12.2 0,14 3.1 FELB-27 2.13 <5 14.4 0.31 3.4 FELB-28 1,98 <5 11.4 0,18 3.5 FELB-29 2.17 <5 13,6 0.29 4.1 FELB-30 2.12 <5 11.5 0.27 3.4 FELB-31 2.22 <5 13.4 0.5 3.1 FELB-32 1,9 <5 5.9 0.16 2.3 STAN DAR 0.02 169 5.2 0.91 6.3 FELB-33 1,13 <5 4.1 0.15 1,5 STAN DAR 0.02 180 5 0.86 6.2
Table 5: (ll4an.!um ~flchs I~ .>olk
ACME ANALYTICAL LABORATORIES LTD. 852 E. HASTINGS ST. VANCOUVI!R BC V6A 1R6 PHO Deep Search Expl. Technologies Inc. Acme file # A406081 Received: OCT 4 2004 * 47 samples in this disk file. Analysis: GROUP 1 F ~ 0.50 GM ELEMENT Mo Cu Pb Zn Ag Ni Co Mn SAMPLES ppm ppm ppm ppm ppb ppm ppm ppm FELS-01 0.32 3.28 3.43 15.8 -10 8.7 2.9 227
FELS-02 0.4 2.84 4.18 14.7 7 8.1 2.8 232
FELS-03 0.18 1.8 2.43 12.3 2 7.3 2.5 87
FELS-04 0.15 2.09 1.95 9.7 3 5.8 2.1 185
FELS-05 0.12 2.9 2.48 17.7 4 8.3 2.5 224
FELS-06 0.14 1.98 1.73 14.6 4 6.7 2 82
FELS-07 0.13 2.58 3.68 15.4 3 7.6 2.2 79
FELS-08 0.14 1.66 2.05 12.4 3 6.8 2 71
FELS-09 0.15 1.93 2.24 12.5 4 7.4 2.1 73
FELS-10 0.39 2.79 3.31 21.2 5 12.8 5.3 308 FELS-11 0.18 1.95 2.06 10.5 3 7.3 2.2 77 FELS-12 0.43 3.73 3.95 15.1 6 12.9 3.9 84 FELS-13 0.19 2.25 4.29 16.4 4 10.3 3 83 FELS-14 0.31 2.98 -.. 7.8 ·.:;.27.5 - 10 11.5 4 102 FELS-15 0.25 2.12 4.37 18.9 8 9.7 3.5 89 FELS-16 0.26 2.99 4.18 17 4 11.8 4.1 87/! RE FELS-1 0.24 2.89 3.97 14.9 5 11.3 3.8 84? FELS-17 0.2 2.54 4.55 16.3 4 12 3.6 102 FELS-18 0.43 3.39 6.13 18.2 8 11.3 3.2 74 FELS-19 0.41 3.22 4.69 12.6 5 10.8 3.3 68 FELS-20 ..... 0.46 -~ 4.92 5.75 18.6 6 -*14.7 4.7 101 FELS-21 0.18 3.91 2.7 14.9 3 12.7 4.1 132 FELS-22 0.2 2.62 3.82 10.4 3 9.4 2.9 65 FELS-23 0.1 1.96 3.97 10.8 <2 12.4 3.3 62 FELS-24 0.38 4 5.09 15.8 8 -~14.3 3.9 74 FELS-25 0.19 2.29 3.83 '13.1 5 6.6 2.2 64 FELS-26 0.18 3.65 3.75 16.4 < 5 11.4 4 92 FE LS-27 0.09 2.08 4.34 7.5 2 f}.1 2.3 46 FELS-28 0.14 2.29 3.09 10.4 3 7.7 2.2 58 FELS-29 0.18 2.8 3.03 10 6 9 2.6 60 FELS-30 0.2 2.12 4.34 13.3 4 8.5 2.6 73 FELS-31 0.33 3.65 ·6.43 14.7 9 --i-.14.7 4.4 117 FELS-32 O.~ 2.89 3.96 13.7 6 10.7 3.2 86 FELS-33 0.26 2.57 5.93 11.9 4 8.7 3.1 80 STAN DAR 12.43 143.96 25.71 139.6 279 25.3 11.9 793 '-.' FELS-34 0.18 3.79 3.86 11.6 4 10.3 3.1 82 FELS-35 0.2 2.33 4.03 14.8 5 8.8 2.7 166 FELS-36 0.32 2.72 5.16 15.1 5 13.2 4.4 148 FELS-37 0.24 2.27 4.2 15.6 7 7.8 2.6 87 FELS-38 0.18 2.31 4.44 19.5 5 9.4 3 204 FELS-39 0.19 1.98 4.84 15.1 <2 7.3 2.5 71 FELS-40 0.12 3.87 2.8 17.8 4 13.3 4.2 152 1 RE FELS-L - 0.14 4.06 2.76 18.3 3 ~ 14.1 4.3 157 J FELS-41 0.23 3.27 4.91 17.2 10 9.8 3.1 66 FELS-42 0.3 3.03 - 6.68 20.4 6 9.1 2.7 82 FELS-43 0.23 1.83 4.54 15.1 4 6.4 2.6 143 FELS-44 0.19 2.79 3.88 13.7 6 9.2 3.1 78 FELS-45 0.13 1.06 2.8 15.8 3 4.3 2.8 -+341 STAN DAR 12.29 144.77 25.36 136.9 281 24.8 11.7 790
NE(604)253-3158 FAX(604)253-1716
ELEMENT Fe As U Au Th Sf Cd Sb
SAMPLES % ppm ppm ppb ppm ppm ppm ppm
FELS-01 1.8 1.2 0.3 4.7 3.2 6.9 0.03 0.05
FELS-02 1.71 1.1 0.3 -:..190.2 2.1 6.6 0.02 0.03
FELS-03 0.97 0.6 0.2 1.3 1.1 5.2 0.02 0.02
FELS-04 0.64 0.6 0.2 0.9 1.2 4.1 0.04 0.03
FELS-05 0.72 0.9 0.2 1.1 2.3 5.6 0.04 <.02
FELS-06 0.75 0.4 0.2 0.3 1.5 5 0.02 0.02
FELS-07 0.61 0.8 0.2 0.9 1.5 4.9 0.04 0.03
FELS-08 0.94 0.6 0.2 0.4 1.4 5.2 0.02 0.02
FELS-09 1.02 0.8 0.1 1.9 1.1 4.6 0.02 0.03
FELS-10 1.52 1.3 0.3 1.1 2.1 ,-. 7.2 0.03 0.04
FELS-11 1.39 0.6 0.1 1.2 1.2 3.8 0.01 0.02
FELS-12 2.08 1.4 0.3 2.3 2.6 4.7 0.04 -0.06
FELS-13 1.82 1 0.2 0.6 2.1 4.6 - 0.07 0.04
FELS-14 2.89 1.4 0.3 ~24.6 2.3 5.3 - 0.07 0.04
FELS-15 1.94 0.8 0.2 0.7 1.8 4.4 0.04 0.02
FELS-16 ,. 1.79 1.2 0.3 0.9 3 4.6 0.04 0.06
RE FELS-1 - 1.73 1.3 0.2 0.6 2.6 4.3 0.03 0.03 ._
FELS-17 2.42 1.1 0.2 0.2 1.9 4.9 0.04 0.03 FELS-18 2.31 1.1 0.2 0.9 1.5 - 8 0.04 0.04 FELS-19 2.11 1.4 0.2 <.2 1.8 5.4 0.04 0.04 FELS-20 2.53 1.5 0.3 0.8 2.3 5.5 - 0.07 0.03 FELS-21 1.44 0.9 0.2 0.4 2 4.8 0.05 0.03 FE LS-22 0.97 0.8 0.3 0.4 2.6 5.3 0.02 0.02 FELS-23 0.66 0.6 0.2 0.5 2.1 - 7.2 0.02 0.02 FELS-24 1.92 - 2.1 0.2 1.1 1.8 5.2 0.03 0.1 FELS-25 1.25 1 0.2 1.2 1.5 5.1 0.04 0.03 FELS-26 1.5 1.1 0.2 1.5 2 4.5 0.02 0.04 FELS-27 0.69 0.6 0.2 2.8 1.5 5.4 0.01 0.02 FELS-28 1.05 0.7 0.1 . 1.6 1.1 4.7 0.01 0.03 FELS-29 1.52 0.9 0.2 <.2 1.7 4.8 0.02 0.02 FELS-30 1.58 1.3 0.2 1.1 1.8 4.6 0.03 0.04 FELS-31 2.19 1.6 0.3 0.8 2.1 6.3 0.02 0.03 FELS-32 1.71 1.2 0.2 2 2 5.3 0.03 0.05 FE LS-33 1~91 1.4 0.3 1.7 2.1 6.3 0.02 0.05 STAN DAR 3.04 17.9 6.4 40.8 2.7 46.6 5.45 3.4 ~ FELS-34 1.96 1.5 0.2 0.9 1.9 5.3 0.02 0.04 FELS-35 1.38 1.1 0.2 0.3 1.8 4.8 0.04 0.06 FELS-36 2.01 1.5 0.2 1 2.2 4.8 0.05 - 0.06 FE LS-37 1.57 0.9 0.2 0.8 2.5 4.3 0.05 0.03 FELS-38 1.55 1 0.2 0.6 1.8 6.2 0.05 0.03 FELS-39 1.G2 1 0.2 0.6 1.5 5.4 0.03 0.02 FELS-40 r 1.36 1.2 0.2 2.2 1.8 5.6 0.04 0.03 -7
RE FELS..L -. 1.4 1.3 0.2 0.7 2 6 0.05 0.03 ;
FELS-41 2.03 1.2 0.2 0.9 1.4 .J
4.1 0.03 0.03 FELS-42 2.36 1.6 0.2 0.3 1.7 4.8 0.03 0.04 FELS-43 1.95 0.9 0.2 0.5 1.9 4.2 0.03 0.03 FE LS-44 1.37 1 0.2 0.2 2.2 5.7 0.03 0.02 FELS-45 1.15 0.4 0.1 0.4 1.5 3.9 0.02 0.03 STAN DAR 2.97 17.6 6.2 42 2.6 46.2 5.46 3.5
ELEMENT Si V Ca P La Cr Mg Sa
SAMPLES ppm ppm % % ppm ppm % ppm
FELS-01 0.05 37 0.17 0.036 4.2 29.6 0.17 26.4
FELS-02 0.06 47 0.18 0.034 4.7 26.8 0.17 39.4
FELS-03 0.03 29 0.14 0.021 3.4 20.2 0.16 11.1
FELS-04 0.04 19 0.08 0.018 4.5 14.5 0.12 12.4
FELS-05 0.04 18 0.18 0.043 5.9 17.7 0.17 14.3
FELS-06 0.03 21 0.14 0.026 4.3 18.6 0.15 11
FELS-07 0.05 15 0.15 0.039 5.4 17.2 0.16 11.3
FELS-08 0.04 27 0.15 0.028 3.3 20 0.15 11.6
FELS-09 0.04 25 0.12 0.027 3.6 20.2 0.16 10.9
FELS-10 0.07 33 0.17 0.023 5.9 31.2 . "- 0.28 22.2
FELS-11 0.04 44 0.08 0.018 3.3 27.4 0.13 7.1
FELS-12 0.07 46 0.09 0.072 4.3 40.7 0.16 18.2
FELS-13 0.08 47 0.09 0.09 4.1 ·34 0.12 22.7
FELS-14 -0.13 ---7 76 0.08 ~-' 0.127 5.1 -, 49.8 0.13 28
FELS-15 0.07 50 0.06 0.101 4.3 38 0.11 18.7
FELS-16 0.07 44 0.09 0.075 4.6 36.6 0.13 20.5 )
RE FELS-1 0.06 42 0.08 0.071 4.6 35.1 0.12 19.4 FELS-17 0.08 72 0.1 0.108 4.3 44.8 0.12 19.8 FELS-18 0.1 56 0.12 0.056 3.9 36.6 0.12 33.1 FELS-19 0.08 48 0.09 0.041 4 35.4 0.14 26.7 FELS-20 0.09 57 0.1 0.044 4.7 45.7 0.17 37.1 FELS-21 0.05 36 0.12 0.047 4.6 33.8 0.16 16.3 FE LS-22 0.06 26 0.11 0.027 4.7 25 0.14 22 FELS-23 0.06 17 0.18 0.039 5.3 19.6 0.19 30 FELS-24 0.09 40 0.08 0.064 4.4 34.3 0.17 21.8 FELS-25 0.07 31 0.07 '0.109 4.8 22.6 0.1 18.6 FELS-26 0.06 35 0.09 --i;, 0.134 4.8 31.8 0.13 18 FELS-27 0.05 20 0.13 0.019 4.2 15.1 0.13 25.9 FELS-28 0.08 36 0.07 • 0.016 3.1 - 23.5 0,11 18.1 FELS-29 0.05 43 0.1 0.092 4.2 33.4 0.1 17.7 FELS-30 0.08 42 0.08 0.09 4.4 27.8 0.1 18.6 FELS-31 0.1 52 0.1 -i' 0.138 5.9 38.9 0.19 30.5 FELS-32 0.07 43 0.1 0.117 4.7 33.3 0.14 21 FELS-33 0.1 51 0.08 0.117 5.3 34.3 0.12 38.1 STAN DAR 6.29 59 0.76 0.093 12.3 183.5 0.69 136.8 X FELS-34 0.07 56 0.12 0.071 4.5 36 0.13 14.6 FELS-35 0.07 34 0.07 0.099 4 24.8 0.11 25.5 FELS-36 0.08 46 0.07 0.092 4.5 35 0.13 28 FELS-37 0.07 37 0.06 0.063 3.9 26.7 0.1 17.1 FELS-38 0.08 35 0.09 - 0.12 4.9 26.8 0.11 40.1 FELS-39 0.09 39 0.07 0.075 4.5 24.3 0.11 24.2 FELS-40 0.05 32 0.12 0.093 5 28.6 0.17 22.4 -1
RE FELS-L 0.05 32 0.13 0.097 5.3 29.9 0.17 22 \ FELS-41 0.08 56 0.06 0.056 3.3 36.2 0.11 23.4 -.J
FELS-42 -~ 0.11 -66 0.06 0.081 3.8 33.3 0.11 21.7 FELS-43 0.08 56 0.05 0.049 3.5 29.5 0.09 17 FELS-44 0.07 31 0.07 0.041 5.5 24.3 0.12 27.8 FE LS-45 0.05 28 0.05 0.071 3.3 18.3 0.06 18.9
. STAN DAR 6.14 58 0.73 0.094 12.2 179.7 0.68 135.2
ELEMENT Ti B AI Na K W Sc TI SAMPLES % ppm % % % ppm ppm ppm FELS-01 0.075 2 1.06 0.011 0.05 <.1 1A 0.04
FELS-02 0.088 2 0.85 0.011 0.04 <.1 1.2 0.04
FELS-03 0.058 2 OA 0.008 0.04 <.1 0.8 0.02
FELS-04 0.043 2 0.39 0.009 0.04 <.1 0.8 0.03
FELS-05 0.038 1 0.38 0.01 0.03 <.1 1 0.03
FELS-06 0.042 2 0.35 0.008 0.03 <.1 0.8 0.02
FELS-07 0.036 1 0.35 0.009 0.03 <.1 0.9 0.03
FELS-08 0.051 1 0.37 0.008 0.03 <.1 0.7 0.02
FELS-09 0.054 1 OA5 0.009 0.04 <.1 0.8 0.03
FELS-10 0.064 1 0.94 0.015 0.06 <.1 1.6 0.05
FELS-11 0.062 2 0.36 0.008 0.03 <.1 0.7 0.02
FELS-12 0.07 2 1.84 0.013 0.06 <.1 1.5 0.04
FELS-13 0.067 ....-..7 1.5 0.012 0.06 <.1 1.3 0.05
FELS-14 0.082 2 ....., 3.03 0.013 0.07 <.1 ~.1 -.;,. 0.07
FELS-15 0.059 2 1.64 0.012 0.06 <.1 1A 0.05 FELS-16 0.063 2 1.72 0.014 0.05 <.1 1.5 0.05 RE FELS-1 0.063 2 1.64 0.012 0.05 <.1 1A 0.05 FELS-17 0.07 5 1.34 0.012 0.05 <.1 1.2 0.04 FELS-18 0.09 2 2.08 0.013 0.06 <.1 1.3 0.05 FELS-19 0.086 2 1.5 0.011 0.05 <.1 1.2 0.04 FELS-20 0.097 2 -2.59 0.014 0.06 <.1 1.7 0.05 FELS-21 0.057 1 1.05 0.01 0.04 <.1 1 0.03 FELS-22 0.071 3 1 0.01 0.04 <.1 1 0.03 FELS-23 0.066 2 1.02 0.012 0.05 <.1 1.2 0.03 FELS-24 0.073 3 1.76 0.013 0.06 <.1 .1.5 0.05 FELS-25 0.056 4 1.11 0.011 0.05 <.1 1.1 0.05 FELS-26 0.056 2 1.17 0.009 0.04 <.1 1.2 0.04 FELS-27 0.045 2 0.65 • 0.01 0.03 <.1 0.9 0.02 FELS-28 0.061 1 0.58 0.009 0.04 <.1 0.8 0.03 FELS-29 0.055 2 0.89 0.008 0.04 <.1 1 0.03 FELS-30 0.066 2 1.03 0.009 0.04 <.1 1.1 0.04 FELS-31 0.066 ~8 1.68 0.014 0.07 <.1 1.6 _." 0.07 FELS-32 0.06,2 3 1.18 0.01 0.05 <;1 1.3 0.04 FELS-33 0.062 3 1.76 0.013 0.06 <.1 1.6 0.06 STAN DAR 0.098 18 2.06 0.034 0.14 5 3.4 1.07 :7~
FE LS-34 0.066 2 0.78 0.01 0.05 <.1 1 0.04 FELS-35 0.049 3 1.1 0.011 0.05 <.1 1 0.05 FELS-36 0.064 2 2.04 0.014 0.06 <.1 1A 0.05 FELS-37 0.059 2 1A8 0.012 0.05 <.1 1.2 0.05 FELS-38 0.054 -7- 8 1A9 0.012 0.05 <.1 1A 0.05 FELS-39 0.063 3 1.1 0.011 0.06 <.1 1.1 0.05 FELS-40 0.048 1 0.98 0.012 0.05 <.1 1.1 0.03 RE FELS-' 0.049 <1 .1.02 0.011 0.05 <.1 1.1 0.04-FELS-41 0.065 1 2.16 0.014 0.07 <.1 1.3 0.05 FELS-42 0.073 1 1.8 0.012 0.07 <.1 1.2 0.06 FELS-43 0.068 1 1.24 0.01 0.06 <.1 1 0.05 FELS-44 0.05 1 1.6 0.011 0.05 <.1 1A 0.04 FELS-45 0.042 1 0.51 0.008 0.05 <.1 0.7 0.03 STAN DAR 0.096 16 2.01 0.034 0.14 4.9 3.3 1.03
ELEMENT S Hg Se Te Ga
SAMPLES % ppb ppm ppm ppm
FELS-01 0.04 7 0.1 <.02 3.5 FELS-02 0.01 10 0.1 <.02 4.7 FELS-03 <.01 13 <.1 <.02 2.4 FELS-04 0.03 7 <.1 <.02 1.9 FELS-05 <.01 9 <.1 <.02 1.4 FELS-06 0.01 10 <.1 <.02 1.6 FELS-07 0.01 10 <.1 <.02 1.4 FELS-08 <.01 6 <.1 <.02 2 FE LS-09 <.01 18 <.1 <.02 2.1 FELS-10 0.02 9 0.1 <.02 3.1 FELS-11 <.01 12 <.1 <.02 2.7 FELS-12 <.01 13 0.2 <.02 4.3 FELS-13 0.01 10 <.1 <.02 5.9 FELS-14 0.01 13 0.2 <.02 -10.1 FELS-15 <.01 13 0.1 <.02 4.9 FELS-16 <.01 9 0.1 <.02 4.3 RE FELS-1 0.01 7 0.1 <.02 4.1 ~. FELS-17 0.01 18 <.1 <.02 5.8 FELS-18 <.01 16 0.2 <.02 7.5 FELS-19 0.01 12 0.1 <.02 5.3 FELS-20 <.01 13 0.1 <,02 6.7 FELS-21 <.01 12 0.1 <.02 2.5 FELS-22 0.02 12 0.1 <.02 3.5 FELS-23 <.01 21 <.1 <.02 4.2 FELS-24 <.01 15 0.2 0.02 5.6 FELS-25 <,01 10 0.1 <.02 4.9 FELS-26 0.01 19 0.1 0.02 3.7 FELS-27 <.01 13 0.1 <.02 2.3 FELS-28 <.01 16 0.1 <.Q2 3.8 FELS-29 <.01 15 0.1 <.02 3.6 FELS-30 <.01 18 0.1 <.02 5.2 FELS-31 <.01 19 0.2 <.02 7.5 FELS-32 <.01 19 0.2 0.02 4.5 FELS-33 0.01 27 0.2 <.02 8.1 STAN DAR 0.02 188 5 0.86 6.5 '.( ...
FELS-34 0.02 <5 0.1 <.02 4.1 FELS-35 0.01 <5 0.2 <.02 4.6 FEL8-36 <.01 <5 0.2 <.02 6 FELS-37 <.01 <5 0.1 <.02 4.7 FELS-38 <.01 <5 0.1 <.02 5.5 FELS-39 <.01 <5 0.1 <.02 6.7 FELS-40 <.01 <5 0.1 <.02 2.7 RE FELS-L <.01 <5 0.1 <.02 2.8 FELS-41 <.01 <5 0.2 0.02 6.8 FELS-42 <.01 <5 0.2 <.02 -!> 10.1 FE LS-43 <.01 <5 0.1 <.02 6.4 FELS-44 <.01 5 0.2 <.02 5 FELS-45 <.01 <5 <.1 <.02 3.7 STAN DAR 0.01 171 4.9 0.87 6.4
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1.11 209.15 118.80 1273.0 514 56.6 4.7 3048 .55 2.3 .2 66.7 .8 295.8 14.10 .92 1.10 12 15.37 .699 3.7 12.4 .57 610.6 .017 113 .46 .024 l.87 .2 .8 .82 .75 <5 2.2 .07 1.2
4.16485.68463.201362.5 613162.9 6.6 3688 1.12 11.0 .7124.0 1.3186.519.965.023.68 3315.241.030 8.3 20.7 .83 150.3.022 1392.25 .037 1.94 .6 1.61.632.16 <512.2 .23 3.0
1.12173.06 91.131165.1 480 39.5 4.2 9514 .56 4.5 .3 35.5 .6455.917.90 .71 .94 1022.17 .625 4.2 10.5 .53 184.6.015 103 .41 .023 2.39 .1 1.1 LOS 1.25 <5 2.5 .07 1.4
1.15177.90 93.881220.3 480 40.3 4.9 9521 .52 4.1 .3 37.5 .6496.615.96 .74 .89 1023.63 .672 4.2 10.4 .52 227.9 .015 113 .38 .0232.30 .1 1.0 1.03 1.17 <5 2.6 .09 1.5
1.33 205.52 llB.93 1344.4 492 50.9 4.1 9933 .40 4.8 .2 62.5 .3677.616.05 .97 1.03 826.72 .651 2.4 5.2 .49 129.3 .008 122 .37 .018 2.32 .1 .7 .521.69 <5 3.4 .12 1.3
FELB-19 2.77 463.38 359.73 1575.3 668 120.5 4.9 6146 .67 6.7 .4338.1 .6686.1 17.873.44 2.52 20 24.79 .994 4.9 17.3 .72 165.0 .013 147 1.68 .0262.57 .3 .9 1.021.71 <5 9.3 .15 2.1
FELB·20 4.40 669.83597.561907.1 980 199.9 6.6 6172 1.15 11.3 .7 155.8 l.l 497.6 29.22 5.384.50 34 21.22 1.269 8.7 32.1 .89 142.2 .020 1612.93 .0362,83 .4 1.7 1.83 2.17 <514.0 .26 3.5
FELB-21 4.51572.15694.11 1907.8 836191.6 6.7 53021.1311.0 .714B.9 1.2483.0 2B.79 5.78 4.56 3720.72 1.251 8.9 22.3 .93 140.5 .020 144 2.95 .0362.34 .5 1.62.202.31 <515_0 .22 3.5
FELB-22 3.42513.17584.891642.4 1342 170.4 5.9 5824 .86 8.7 .5286.5 .9532.722.90 4.313.37 2722.921.196 7.1 18.9 .89 150.9.016 1192.25.0303.03 .4 1.31.672.11 <512.4 .25 2.5
fELB-23 2.89726.17442.531675.6 564 122.4 4.8 6677 .66 7.1 .4 548.1 .7515.024,883.36 2.75 21 23.59 l.023 5.4 75.7 .93 135.9 .012 1342.11 .0302.63 .4 1.0 .731.89 <510.1 .19 1.9
FELB-Z4 3.73442.48530.311469.9 787127.6 5.4 4978 .90 9.9 _5229.7 1.1 373.8 18.244.814.10 2722.781.098 6.8 19.9 .81 144.2.016 1431.73.043 2.81 .4 1.41.171.98 <512.4 .20 2.7
FELB-25 4.89 542.80 698.41 1632.9 907 141.2 5.9 5035 1.11 11.1 .6678.0 1.5 262.121.646.014.84 3420.981.272 8.3 24.8 .99 139.8 .018 1492.28 .0502.77 .6 1.5 1.632.10 <5 13.1 .23 3.1
FELB-26 4.27504.54 585.89 1572.4 875 138.0 5.4 5738 1.10 10.1 .6401.0 1.2285.321.28 5.24 4.47 3322.47 1.179 7.9 26.91.02 167.0 .018 1492.21 .0482.64 .4 1.6).492.09 <512.2 .14 3.1
FElB·27 5.65 649.39 693.471642.61021205.5 7.5 5238 1.26 12.0 .7241.3 1.6322.119.765.935.53 3722.211.170 8.8 2B.6 .92 143.3.019 1602.22 .046 2.42 .6 1.6 1.75 2.13 <514.4 .31 3.4
FELB·2S 5.09445.41523.77 1476.7 865 157.6 6.3 362D 1.22 8.1 .7310.2 1.7380.4 14.914.993.95 3321.401.010 9.2 30.8 .85 138.3 .020 1791.93 .0462.40 .5 1.81.35 1.98 <5 11.4 .18 3.5
FElB·29
FELB-30
FElB-31
FELB-32
ST ANDAAll 055
5.52575.49624.921633.51044205.4 7.4 7416 l.2210.0 .8276.3 1.5 415.5 21.97 5.76 4.86 3B 21.94 1.038 9.4 30.9 .80 129.0.021 1851.79.0452.72 .6 1.7 .992.17 <513.6 .29 4.1
4.43524.53540.01 1674.3 961 195.5 6.8 9489 1.05 9.7 .6151.9 1.2 455.4 23.72 4.63 3.90 3224.65 .961 7.7 23.8 .77 130.5 .017 189 1.79 .0382.44 .4 1.4 1.062.12 <5 1l.5 .27 3.4
5.06681.71613.36 1772.2 1036 274.2 B.8 4790 1.25 9.5 .6176.7 1.6373.025.974.515.56 3423.401.097 8.9 24.6 .89 166.4 .019 1692.22 .0472.66 .7 1.5 1.222.22 <5 13.4 .50 3.1
2.59404.30319.39 1642.8 964 140.9 5.311338 .68 7.8 .4162.1 .7566.1 24.83 2.702.54 1925.991.066 4.7 16.5 .71 165.7 .013 180 1.17 .0312.93 .3 1.0 1.71 1.90 <5 5.9 .16 2.3
12.41142.00 24.00 140.0 272 26.211.1 8183.0418.2 6.2 45.0 2.6 44.8 5.503.496.16 59 .78 .10313.2181.0 .70 137.3.105 172.00.037 .15 5.4 3.41.08 .02 169 5.2 .91 6.3
GROUP 1F - 0.25 GM SAMPLE LEACHED WITH 3 ML 2-2-2 HCL-HN03-H20 AT 95 DEG. C FOR ONE HOUR, DILUTED TO 10 ML, AN (» CONCENTRATION EXCEEOS UPPER LIMITS. SOME MINERALS MAY BE PARTIALLY ATTACKED. REFRACTORY AND GRAPHITIC - SAMPLE TYPE: BRK ASH Samples beginning 'RE' are Reruns and 'RRE' are Reject Reruns.
OCT 4 2004 DATE REPORT MAILED, /P ~ !-? r.y. Data--L.t FA JUN 1 3 2005 ~l.-~=S~;:;;+.-. DATE RECEIVED:
GEOSCIENCE ASSESSMEN
All results are considered the confidential property of the client. Acme the liabilities for actual cost~~oT-~~~~"
SAMPLE# Mo ppm
Cu ppm
Pb ppm
Deep Search Expl. Technologies Inc.
Zn Ag Ni Co ppm ppb ppm ppm
Mn ppm
Fe As U % ppm ppm
Au Th ppb ppm
Sr ppm
Cd Sb Bi V ppm ppm ppm ppm
Ca %
FILE # A406082
P La % ppm
Cr Mg ppm %
Ba ppm
Ii B % ppm
Al Na % %
Page 2
K W Sc T1 % ppm ppm ppm
tt S Hg Se Te Ga % ppb ppm ppm ppm
FELB-33 1.80279.21 249.191853.8510 87.5 4.1 12129 .36 5.2 .2 256.3 .3 935.0 21.90 1.93 1.58 12 29.26 .704 2.9 9.7 .69 232.2 .007 189 .69 .0222.44 .2 .6 .52 1.13 <54.1 .15 1.5 STANDARD 12.34 142.59 24.72 140.6 278 24.2 11.2 8022.99 16.9 6.0 41.6 2.7 44.3 5.56 3.41 5.75 60 .77 .091 12.8 176.2 .65 135.5 .104 17 2.02 .036 .14 5.3 3.4 1.05 .02 180 5.0 .866.2
Standard is STANDARD 055.
All results are considered the confidential property of the client. Acme assumes the liabilities for actual cost of the analysis only.
SAMPLE4/ Mo Cu Pb Zn Ag Ni Co Mn Fe {ls U Au Th Sr Cd Sb 8i V Ca P La Cr Mg Ba Ti B Al Na K I~ Sc Tl S Hg Se Te Ga ppm ppm ppm ppm ppb ppm ppm ppm % ppm. ppm ppb ppm ppm ppm ppm ppm ppm % % ppm ppm % ppm % ppm % % % ppm ppm ppm % ppb ppm ppm ppm
FELS-01 .32 3.28 3.43 15.8 10 8.7 2.9 227 1.80 1.2 .3 4.73.2 6.9 .03 .05 .05 37 ,17 .036 4.2 29.6 ,17 26.4 .075 2 1.06 .011 .05 <.1 1.4 .04 .04 7 .1<.02 3.5 FELS-02 .40 2.84 4.18 14.7 7 8,1 2.8 232 1.71 1.1 .3 190.2 2.1 6.6 .02 .03 .06 47 .18 ,034 4.7 26.8.17 39.4 .088 2 .85 .011 .04 <.1 1.2 .04 .01 10 .1<.02 4.7 FELS-03 .18 1.80 2.43 12.3 2 7.3 2.5 87 ,97 .6 .2 1.31.1 5.2 .02 .02 .03 29 .14 .021 3.4 20.2 .16 11.1 .058 2 .40 .008 .04 <.1 .8 .02<.01 13'.'"<.1<.02 2.4 FELS-04 .15 2.09 1.95 9.7 3 5.8 2.1 185 .64 .6 .2 ,9 1.2 4,1 .04 ,03 .04 19 .08 .018 4.5 14.5 .12 12.4 .043 2 .39 .009 .04 <.1 .8 .03 .03 7 ·;tj:';.02 1.9 FELS-05 .12 2.90 2.48 17.7 4 8.3 2.5 224 .72 .9 ,2 l.1 2.3 5.6 .04 <.02 .04 18 .18 .043 5.9 17.7 .17 14.3 .038 1 .38 .010 .03 <.1 1.0 .03<.01 9 <.1<.02 1.4
FELS-06 ,14 1.98 1.73 14.6 4 6.7 2.0 82 .75 .4 .2 .3 1.5 5.0 .02 .02 .03 21 .14 .026 4.3 18.6 .15 11.0 .042 2 .35 .008 .03 <.1 .8 .02 .01 10 <.1<.02 1.6 FELS-07 .13 2.58 3.68 15.4 3 7.6 2.2 79 .61 .8 .2 .91.5 4.9 .04 .03 .05 15 .15 .039 5.4 17.2 .16 11.3 .036 1 .35 .009 .03 <.1 .9 .03 .01 10 <.1<.02 1.4 FELS-08 .14 1.66 2.05 12.4 3 6.8 2,0 71 .94 .6 .2 .41.4 5.2 .02 .02 .04 27 .15 .028 3.3 20.0 .15 11.6 .051 1 .37 .'008 .03 <.1 .7 .02<.01 6 <.1<.02 2.0 FELS-09 .15 1.93 2.24 12.5 4 7.4 2.1 73 1.02 .8 .1 1.9 1.1 4.6 .02 .03 .04 25 .12 .027 3.6 20.2 .16 10.9 .054 1 .45 .009 .04 <.1 .8 .03<.01 18 <.1<.02 2.1 FELS-I0 .39 2.79 3.31 21.2 5 12.B 5.3 308 1.52 1.3 .3 1.1 2.1 7.2 .03 .04 .07 33 .17 .023 5.9 31.2 .28 22.2 .064 1 .94 .915 .06 <.1 1.6 .05 .02 9 .1<.02 3.1
FELS-ll .18 1.95 2.06 10.5 3 7.3 2.2 77 1.39 .6 .1 1.2 1.2 3.B ,01 .02 .04 44 .08 .018 3.3 27.4 .13 7.1 .062 2 .36 .008 .03 <.1 .7 .02<.01 12 <.1<.02 2.7 FELS-12 .43 3.73 3.95 15.1 6 12.9 3.9 84 2.08 1.4 .3 2.3 2.6 4.7 .04 .06 .07 46 .09 .072 4.3 40.7 .16 18.2 .070 2 1.84 .013 .06 <.1 1.5 .04<.01 13 .2<.02 4.3 FELS·13 .19 2.25 4.29 16.4 4 10.3 3.0 83 1.82 1.0 .2 .6 2.1 4.6 .07 .04 .08 47 .09 .090 4.1 34.0 .12 22.7 .067 7 1.50 .012 .06 <.1 1.3 .05 .01 10 <.1<.02 5.9 FELS-14 .31 2.98 7.BO 27.5 10 11. 5 4.0 102 2.89 1.4 .3 24.6 2.3 5.3 .07 .04 .13 76 .08 .127 5.1 49.8 .13 2B.0 .082 2 3.03 .013 .07 <.1 2.1 .07 .01 13 .2<.0210.1 mS-15 .25 2.12 4.37 18.9 8 9.7 3.5 89 1.94 .8 .2 .71.B 4.4 .04 .02 .07 50 .06 .101 4.3 38.0 .11 18.7 .059 2 1.64 .012 .06 <.1 1.4 .05<.01 13 .1<.02 4.9
FELS-16 .26 2.99 4.18 17.0 4 11.8 4.1 87 1. 79 1.2 .3 .9 3.0 4.6 .04 .06 .07 44 .09 .075 4.6 36.6 .13 20.5 .063 2 1.72 .014 .05 <.1 1.5 .05<.01 9 .1<.02 4.3 RE FELS-16 .24 2.89 3.97 14.9 5 11.3 3.8 84 1. 73 1.3 .2 .6 2.6 4.3 .03 .03 .06 42 .OB .071 4.6 35.1 .12 19.4 .063 2 1.64 .012 .05 <.1 1.4 .05 . 01 7 .1<.02 4.1 FELS-17 .20 2.54 4.55 16.3 4 12.0 3.6 102 2.42 1.1 .2 .2 1. 9 4.9 .04 .03 .08 72 .10 .10B 4.3 44.B .12 19.8 ,070 5 1.34 .012 .05 <.1 1.2 .04 .01 18 <.1<.02 5.8 FELS-1B .43 3.39 6.13 18.2 8 11.3 3.2 74 2.31 l.1 .2 .9 1.5 8.0 .04 .04 .10 56 .12 .056 3.9 36.6 .12 33.1 .090 2 2.08 .013 .06 <.1 1.3 .05<.01 16 .2<.02 7.5 FELS-19 .41 3.22 4.69 12.6 5 10.8 3.3 682.11 1.4 .2 <.2 1.8 5.4 .04 .04 .08 48 .09 .041 4.0 35.4 .14 26.7 .086 2 1.50 .011 .05 <.1 1.2 .04 ,01 12 .1<.02 5.3
FELS-20 .46 4.92 5.75 18.6 6 14.7 4.7 101 2.53 1.5 .3 .82.3 5.5 .07 .03 .09 57 .10 .044 4.7 45.7 .17 37.1 .097 22.59 .014 .06 <.1 1.7 .05<.01 13 .1<.02 6.7 FELS-21 .18 3.91 2.70 14.9 3 12.7 4.1 132 1.44 .9 .2 .4 2.0 4.8 .05 .03 .05 36 .12 .047 4.6 33.8 .16 16.3 .057 1 1.05 .010 .04 <.1 1.0 .03<.01 12 .1<.02 2.5 FELS-22 .20 2.62 3.82 10.4 3 9.4 2.9 65 .97 .8 .3 .4 2.6 5.3 .02 .02 .06 26 .11 .027 4.7 25.0 .14 22.0 .071 3 1.00 .010 .04 <.1 1.0 .03 .02 12 .1<.02 3.5 FELS-23 .10 1.96 3.97 10.8 <2 12.4 3.3 62 .66 .6 .2 .52.1 7.2 .02 .02 .06 17 .18 .039 5.3 19.6 .19 30.0 .066 2 1.02 .012 .05 <.1 1.2 .03<.01 21 <.1<.02 4.2 FELS-24 .38 4.00 5.09 15.B 8 14.3 3.9 74 1.92 2.1 .2 l.1 1.8 5.2 .03 .10 .09 40 .08 .064 4.4 34.3 .17 2l.8 .073 3 1.76 .013 .06 <.1 1.5 .05<.01 15 .2 .02 5.6
FELS-25 .19 2.29 3.83 13.1 5 6.6 2.2 64 1. 25 1.0 .2 1.2 1.5 5.1 .04 .03 .07 31 .07 .109 4.8 22.6 .10 18.6 .056 4 1.11 .011 .05 <.1 1.1 .05<.01 10 .1<.02 4.9 FELS-26 .18 3.65 3.75 16.4 5 11.4 4.0 92 1.50 1.1 .2 1.5 2.0 4.5 .02 .04 .06 35 .09 .134 4.8 31.8 .13 18.0 .056 2 1.17 .009 .04 <.1 1.2 .04 .01 19 .1 .02 3.7 FELS-27 .09 2.08 4.34 7.5 2 8.1 2.3 46 .69 .6 .2 2.8 1.5 5.4 .01 ,02 .05 20 .13 .019 4.2 15.1 .13 25.9 .045 2 .65 .010 .03 <.1 .9 .02<.01 13 .1<.02 2.3 FELS-28 .14 2.29 3.09 10.4 3 7.7 2.2 58 1. 05 .7 .1 1.61.1 4.7 .01 .03 .08 36 .07 .016 3.1 23.5 .11 18.1 .061 1 .58 .009 .04 <.1 .8 .03<.01 16 .1<.02 3.8 FELS-29 .18 2.80 3,03 10.0 6 9.0 2.6 60 1. 52 .9 .2 <.2 1.7 4.8 .02 .02 .05 43 .10 .092 4.2 33.4 .10 17.7 .055 2 .89 .OOB .04 <.1 1.0 .03<.01 15 .1<.02 3,6
FELS-30 .20 2.12 4.34 13.3 4 8.5 2.6 73 1.58 1.3 .2 1.1 1.8 4.6 .03 .04 .08 42 .08 .090 4.4 27.8 .10 18.6 .066 2 1.03 .009 .04 <.1 1.1 .04<.01 18 .1<.02 5.2 FELS-31 .33 3.65 6.43 14.7 9 14.7 4.4 117 2.19 1.6 .3 .B 2.1 6.3 .02 .03 .10 52 .10 .138 5.9 38.9 .19 30.5 ,066 8 1.68 .014 .07 <.1 1.6 .07<.01 19 .2<.02 7.5 FELS-32 .22 2.89 3.96 13.7 6 10.7 3.2 86 1. 71 1.2 .2 2.0 2.0 5.3 .03 .05 .07 43 .10 .117 4.7 33.3 .14 21.0 .062 3 1.18 .010 .05 <.1 1.3 .04<.01 19 .2 .02 4.5 FELS-33 .26 2.57 5.93 11.9 4 8.7 3.1 80 1.91 1.4 .3 1.72.1 6.3 .02 .05 .10 51 .08 .117 5.3 34.3 .12 38.1 .062 3 1.76 .013 .06 <.1 1.6 .06 .01 27 .2<.02 8.1 STANDARD DS5 12.43143.9625.71 139.627925.311.97933.04 17.9 6.4 40.8 2.7 46.6 5.45 3.40 6.29 59 .76 .093 12.3 183.5 .69 136.8 .098 1B 2.06 .034 .14 5.0 3.4 1.07 .02 188 5.0 .86 6.5
GROUP 1F - 0.50 GM SAMPLE LEACHED WITH 3 ML 2-2-2 HCL-HN03-H20 AT 95 DEG. C FOR'.ONE HOUR, DILUTED TO 10 ML, ANALYSED BY ICP/ES & MS. (» CONCENTRATION EXCEEDS UPPER LIMITS. SOME MINERALS MAY BE PARTIALLY ATTACKED. REFRACTORY AND GRAPHITIC SAMPLES CAN LIMIT AU SOLUBILITY - SAMPLE TYPE: SOIL PULP , ... l,. beg'"";n. -.,- '" ","n' '"' -'''- '" "'I'" "'""'~~ ~ Data-'...t FA __
;,~ . () DATE RECEIVED: OCT 4 2004 DATE REPORT MAILED: "~' •••• ltJ .. ff. ...
All results are considered the confidential operty of the client. Acme assumes the liabilities for actual cost of the analysis only.
[tic' I
.. Deep Search Expl. Technologies Inc . FILE # A406081 Page 2 tt ACME ANAL YTlCIIL
SAMPLE# Ho Cu Pb Zn Ag Ni Co Mn Fe As U Au Th Sr Cd Sb Bi V Ca P La Cr Hg Ba Ti B Al Na K W Sc T1 S Hg Se Te Ga ppm ppm ppm ppm ppb ppm ppm ppm % ppm ppm ppb ppm ppm ppm ppm ppm ppm % % ppm ppm % ppm % ppm % % % ppm ppm ppm % ppb ppm ppm ppm
FELS-34 .18 3.79 3.B6 11.6 4 10.3 3.1 821.96 1.5 .2 .91.9 5.3 .02 .04 .07 56 .12 .071 4.5 36.0 .13 14.6 .066 2 .78 .010 .05 <.1 1.0 .04 .02 <5 .1<.02 4.1 FELS-35 .20 2.33 4.03 14.8 5 8.8 2.7 166 1.38 1.1 .2 .3 1.8 4.8 .04 .06 .07 34 .07 .099 4.0 24.8 .11 25.5 .049 3 1.10 .011 .05 <.1 1.0 .05 .01 <5 .2<.02 4.6 FELS-36 .32 2.72 5.16 15.1 5 13.2 4.4 148 2.01 1.5 .2 1.0 2.2 4.8 .05 .06 .08 46 .07 .092 4.5 35.0 .13 28.0 .064 2 2.04 .014 .06 <.1 1.4 .05<.01 <5 .2<.02 6.0 FELS-37 .24 2.27 4.20 15.(} 7 7.8 2.6 87 1. 57 .9 .2 .8 2.5 4.3 .05 .03 .07 37 .06 .063 3.9 26.7 .10 17.1 .059 2 1.48 .012 .05 <.1 1.2 .05<.01 <5 .1<.02 4.7 FELS-3B .18 2.31 4.44 19.5 5 9.4 3.0 204 1.55 1.0 .2 .6 1.8 6.2 .05 .03 .08 35 .09 .120 4.9 26.8 .11 40.1 .054 8 1.49 .012 .05 <.1 1.4 .05<.01 <5 .1<.02 5.5
FELS-39 .19 1.98 4.84 15.1 <2 7.3 2.5 71 1.52 1.0 .2 .6 1.5 5.4 .03 .02 .09 39 .07 .075 4.5 24.3 .11 24.2 .063 31.10 .011 .06 <.1 1.1 .05<.01 <5 .1<.02 6.7 FELS-40 .12 3.87 2.80 17.8 4 13.3 4.2 152 1.36 1.2 .2 2.2 1.8 5.6 .04 .03 .05 32 .12 .093 5.0 28.6 .17 22.4 .048 1 .98.012.05 <. 1 1.1 .03<.01 <5 .1<.02 2.7 RE FELS-40 .14 4.06 2.76 18.3 3 14.1 4.3157 1.40 1.3 .2 .7 2.0 6.0 .05 .03 .05 32 .13 .097 5.3 29.9 .17 22.0 .049 <1 1.02 .011 .05 <.1 1.1 .04<.01 <5 .1<.02 2.8 FELS-41 .23 3.27 4.91 17.2 10 9.8 3.1 66 2.03 1.2 .2 .9 1.4 4.1 .03 .03 .08 56 .06 .056 3.3 36.2 .11 23.4 .065 1 2.16 .014 .07 <.1 1.3 .05<.01 <5 .2 .02 6.8 FELS-42 .30 3.03 6.68 20.4 6 9.1 2.7 82 2.36 1.6 .2 .3 1.7 4.8 .03 .04 .11 66 .06 .081 3.8 33.3 .11 21. 7 .073 1 1.80 .012 .07 <.1 1.2 .06<.01 <5 .2<.02 10.1
FELS-43 .23 1.83 4.54 15.1 4 6.4 2.6 143 1.95 .9 .2 .5 1.9 4.2 .03 .03 .08 56 .05 .049 3.5 29.5 .09 17.0 .068 1 1.24 .010 .06 <.1 1.0 .05<.01 <5 .1<.02 6.4 FELS-44 .19 2.79 3.88 13.7 6 9.2 3.1 78 1.37 1.0 .2 .2 2.2 5.7 .03 .02 .07 31 .07 .041 5.5 24.3 .12 27.8 .050 1 1.60 .011 .05 <.1 1.4 .04<.01 5 .2<.02 5.0 FELS-45 .13 1.06 2.80 15.8 3 4.3 2.8341 1.15 .4 .1 .4 1.5 3.9 .02 .03 .05 28 .05 .071 3.3 18.3 .06 18.9 .042 1 .51 .008 .05 <.1 .7 .03<.01 <5 <.1<.02 3.7 STANDARD DS5 12.29 144.77 25.36 136.9281 24.8 11.7 7902.97 17.66.242.02.646.25.463.50 6.14 58 .73 .094 12.2 179.7 .68 135.2 .096 162.01 .034 .144.93.3 1.03 .01 1714.9 .87 6.4
Sample type: SOIL PULP. Samples beginning 'RE' are Reruns and 'RRE' are Reject Reruns.
All results are considered the confidential property of the client. Acme assumes the liabilities for actual cost of the analysis only. Data.LFA __
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GE:OLOGY
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JULY, 200'3; .AUGUST, 2°olf
Scale 1 : 10 000 }
NAP 3
